[ 43 J 



Bohemian or fouthern fide Charpent, p. 75. The fouthern dci- 

 clivity IS to the northern as fix to two, 2d Bergm. Journ. 1792, 

 p. 384 and 385. 



7** The mountains which feparate Silefia from Bohemia run 

 nearly from E. to W. yet are fteeper on the norihern or Silefian 

 fide than on the oppofite Bohemian, Affemanni Silefia, 335. Such 

 branches as run from N. E. to S. W. have their weftern covered 

 with primordial ftrata and confequently lefs fteep, 4, New Roz. 



P- 157' 



8° The Meiflener in Heflia is fleeper on the N. and E. fides 

 which face the Warra than on the fouth and weftern, i, Bergm. 

 Journ. 1789, p. 272. 



9" The mountains of the Hartz and Habichtswald are fteep 

 on the fouth and gentle on the northern fides, Fofter § 46. 



10° The Pyrenees which run from E. to W. are fteeper on 

 the fouthern or Spanifii fide, Carbonieres XIII. 



1 1*' The mountains of Crim Tartary are gentle on the northern 

 and fteep on the fouthern fides, Fofter, ibid. 



In j^Jia. 



12*^ The Ourals which ftretch from N. to S. are far fteeper on. 

 weftern than on the fouthern fides,. Herman Geologic, p. 90, and 

 2d Ural Befchreib. p. 389. 



F 2 13" The 



